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海底弧火山的长期喷发活动。

Long-term eruptive activity at a submarine arc volcano.

作者信息

Embley Robert W, Chadwick William W, Baker Edward T, Butterfield David A, Resing Joseph A, de Ronde Cornel E J, Tunnicliffe Verena, Lupton John E, Juniper S Kim, Rubin Kenna H, Stern Robert J, Lebon Geoffrey T, Nakamura Ko-ichi, Merle Susan G, Hein James R, Wiens Douglas A, Tamura Yoshihiko

机构信息

NOAA/PMEL, 2115 SE O.S.U. Drive, Newport, Oregon 97365-5258, USA.

出版信息

Nature. 2006 May 25;441(7092):494-7. doi: 10.1038/nature04762.

Abstract

Three-quarters of the Earth's volcanic activity is submarine, located mostly along the mid-ocean ridges, with the remainder along intraoceanic arcs and hotspots at depths varying from greater than 4,000 m to near the sea surface. Most observations and sampling of submarine eruptions have been indirect, made from surface vessels or made after the fact. We describe here direct observations and sampling of an eruption at a submarine arc volcano named NW Rota-1, located 60 km northwest of the island of Rota (Commonwealth of the Northern Mariana Islands). We observed a pulsating plume permeated with droplets of molten sulphur disgorging volcanic ash and lapilli from a 15-m diameter pit in March 2004 and again in October 2005 near the summit of the volcano at a water depth of 555 m (depth in 2004). A turbid layer found on the flanks of the volcano (in 2004) at depths from 700 m to more than 1,400 m was probably formed by mass-wasting events related to the eruption. Long-term eruptive activity has produced an unusual chemical environment and a very unstable benthic habitat exploited by only a few mobile decapod species. Such conditions are perhaps distinctive of active arc and hotspot volcanoes.

摘要

地球上四分之三的火山活动发生在海底,主要集中在大洋中脊,其余的则沿着洋内弧和热点分布,深度从大于4000米到接近海面不等。大多数对海底火山喷发的观测和采样都是间接的,是从水面船只上进行的,或者是在喷发之后进行的。我们在此描述了对一座名为西北罗塔-1的海底弧火山喷发的直接观测和采样,该火山位于罗塔岛(北马里亚纳群岛联邦)西北60公里处。2004年3月以及2005年10月,我们在水深555米(2004年的深度)的火山山顶附近,观测到一股脉动的羽状物,其中充满了熔融硫滴,从一个直径15米的坑中喷出火山灰和火山砾。2004年在火山侧翼700米至1400多米深处发现的一个浑浊层,可能是由与喷发相关的大规模滑坡事件形成的。长期的火山喷发活动产生了一种不同寻常的化学环境和一个非常不稳定的底栖生物栖息地,只有少数几种能移动的十足目物种利用这里的环境。这种情况可能是活跃的弧火山和热点火山所特有的。

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